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Jökull - 01.12.1988, Qupperneq 49

Jökull - 01.12.1988, Qupperneq 49
Explanations (cont.) / Skýringar (frh.): c C Estimated water consumption 1986 of public waterworks (c) and fish farms (C) 70 - 150 1/s / Aætluð vatnsnotkun (1986) vatnsveitna (c) og fiskeldisstöðva (C) 70 -150 lls. d D Estimated water consumption 1986 of public waterworks (d) and fish farms (D) 200 - 700 1/s / Áœtluð vatnsnotkun (1986) vatnsveitna (d) og fiskeldisstöðva (D) 200 - 700 l/s. e E Estimated water consumption 1986 of public waterworks (e) and fish farms (E) > 1,000 1/s / Áœtluð vatnsnotkun (1986) vatnsveitna (e) ogfiskeldisstöðva (E) > 1000 l/s. consequently no leakage. Additional 10 to 20 1/inh.xday can be approximated for the watering of animals during the winter. Surface water was com- mon as a source, as shown by the term "bæjarlækur" (farm brook), which was considered as belonging naturally to every farm. In a survey made in Reykjavík in the year 1903 the water consumption was found to be about 18 1/inh.xday (Kristjánsson, 1952). The water was taken in buckets, mostly from dug wells, and carried or driven in carts to the houses. At that time 40 1/inh.xday were considered as quite adequate in cities abroad. Growth of villages and towns — In Fig. 8 the development of present time predominantly urban society is depicted (Hagstofa íslands, 1984; Fjár- mála og hagsýsludeild Reykjavíkurborgar, 1987). The rural society begins to lose ground in the later half of the last century, but is still prevailing up to the first two or three decades of this century. As people move to urban dwellings, there can be seen a simultaneous development towards a concentration in the southwestem part of the country, in the capital Reykjavík and on the Reykjanes Peninsula. During this time the first water works were built in Iceland, in 1900 in the fishing village of Isafjörður in the northwest, in 1903 in Seyðisfjörður in the east (Björnsson, 1979), in 1904 in Hafnar- fjörður south of Reykjavík, also a fishing village, and in 1908/09 in Reykjavík (Kristjánsson, 1952). At first the water was predominantly for household use, but soon it was also taken for industrial uses, such as washing for the production of salted fish. Higher standard — Economically and socially the first decades of this century meant a completely new way of life for thousands of people. One of the things that changed was the means of getting water, now it came through a pipe and from the tap - not from the farm brook. And people needed much more of the water than before. It was used for WCs, heat- ing elements, washing, bathing etc., many of which were new uses. This placed a heavy burden on many municipalities, because in many places, especially in the northwest and the east, the search for ade- quate groundwater met with small success. Some of the villages had to use surface water, which besides being of questionable quality often became scarce during the wintertime. At the same time the water was considered as having to be inexpensive; every- body was accustomed to having it free of charge in the old society. In 1930 the consumption had risen to about 300 1/inh.xday in Reykjavík, or more than fifteen times the consumption in 1903 (Kristjánsson, 1952), and in 1983 the average water consumption in Reykjavík was nearly 900 1/inh.xday (Vatnsveita Reykjavíkur, Vatnsbólanefnd, 1983), see Fig. 9. The fish industries — As in all other food industry cleanliness and hygienic measures are of prime importance in the fish industry. And that means plenty of water. Accordingly, the demand for ample, good water is of great concem in all fishing villages and towns. The different methods of handling the fish are also of importance. Production of salted fish, as was most common for many decades in the last and the beginning of the present century, doesn’t require as much water as the production of frozen fish. Looking at the increase in production of frozen fish shown in Fig. 10 (Þjóðhagsstofnun, 1987; Hag- stofa Islands, 1984), and bearing in mind that qual- ity demands increased simultaneously, one can see that the need for groundwater must have increased JÖKULL, No. 38, 1988 47
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